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John Stone is an Associate Professor specializing in geology and geochemistry, focusing on cosmic-ray-produced nuclides, which are rare isotopes generated by the bombardment of rocks and soil by cosmic rays. His research involves using the accumulation of these nuclides to date glacial deposits worldwide, including Antarctica, and to establish the history of ice ages and the susceptibility of glaciers and ice sheets to climate change. Dr. Stone employs cosmic-ray-produced nuclides to investigate geomorphic processes, such as erosion and sediment transport, and has conducted fieldwork in diverse geographical regions, including Australia, South America, Asia, and the Pacific Northwest.
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